DOCSLIB.ORG

Intertidal Biota of Te Matuku Bay, Waiheke Island, Auckland

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

Tane 36: 67-84 (1997) INTERTIDAL BIOTA OF TE MATUKU BAY, WAIHEKE ISLAND, AUCKLAND Bruce W. Hayward, A. Brett Stephenson, Margaret S. Morley, Nancy Smith, Fiona Thompson, Wilma Blom, Glenys Stace, Jenny L. Riley, Ramola Prasad and Catherine Reid Auckland Museum, Private Bag 92018, Auckland SUMMARY Ninety-seven Mollusca (7 chitons, 52 gastropods, 38 bivalves), 33 Crustacea (8 amphipods, 4 barnacles, 18 decapods) 10 Echinodermata (3 echinoids, 3 asteroids, 3 ophiuroids, 1 holothurian), 21 Polychaeta and 31 other animals and plants are recorded from Te Matuku Bay, on the south-east corner of Waiheke Island, Auckland. The intertidal communities and their constituent fauna and flora are similar to those encountered around the middle and upper Waitemata Harbour, except for the abundance at Te Matuku Bay of the tube worm Pomatoceros caeruleus. This species used to be equally abundant on Meola Reef but has now disappeared from there. The Pacific oyster is well established on the rocks around Te Matuku Bay, but other introduced organisms (Musculista senhousia, Limaria orientalis, Codium fragile tomentosoides) are present in only small numbers. Keywords: New Zealand; Waiheke Island; Te Matuku Bay; intertidal ecology; Mollusca; Polychaeta; Crustacea; Amphipoda; Decapoda. INTRODUCTION Te Matuku Bay (latitude 36°50'S, longitude 175°08'E) lies on the sheltered south coast of Waiheke Island, near its eastern end (Fig. 1). The bay is long and relatively narrow (2.5 x 1km) and opens to the south into the east end of Tamaki Strait. Both sides of the bay rise relatively steeply to 60-100m high ridge lines. These adjacent slopes are mostly in regenerating scrub, although partly in grazed grassland and partly in mature coastal forest (middle point on eastern side). Several streams draining catchments with a similar mix of uses flow into the head of the bay. Around the edge of the bay, dwellings and baches are restricted to Pearl Bay in the east and two farm cottages on the west side near the mouth. An old oyster farm is present on the sand flats on the west side of the bay. 67 Fig. 1. Te Matuku Bay lies at the south-eastern end of Waiheke Island, inner Hauraki Gulf. 68 The southern quarter of the bay (c. 70ha) is subtidal with a coastline of greywacke rocks and gravel beaches. The middle half of the bay (c. 150ha) is intertidal muddy and shelly sand flats fringed by sandy pebble gravel beaches at high tide level. Muddy mangrove forest covers the remaining quarter (c. 50ha) at the head of the bay. Two sandy shell spits have built out across embayments on the eastern side of the muddy sand flats. The larger provides roosting areas for waders and supports nesting New Zealand dotterel. The Te Matuku Bay area was chosen for study at the invitation of the Royal Forest and Bird Society, who are investigating the site as a possibility for a marine reserve application. Our study was designed to document the intertidal biota of their selected area, which also includes a subtidal portion extending out through the mouth of the bay to Passage Rock. This paper records the biota that was found intertidally in Te Matuku Bay and the rocky points on either side, on a five hour Auckland Museum field trip by most of the authors during a spring low tide in September 1996. Field work included mapping the distribution of the major intertidal communities (Fig. 1), extensive searching of the range of intertidal habitats present in the bay, beach combing around the mid and high tide beaches and digging and dip netting in the muddy sand, especially around low tide level. All records are supported by voucher specimens in the collections of the Auckland Museum (AK). SPECIES LIST Habitat where found (Fig. 2): ir = inner bay rocks s = sand and mud flats m = mangroves ss = subtidal sea floor (wash-up) or = outer bay rocks and gravels d = only seen dead 1 = seen alive Double letter = common Molluscan nomenclature follows Spencer & Willan (1995). m s ir or ss MOLLUSCA - POLYPLACOPHORA Acanthochitona (Notoplax) violacea (Quoy & Gaimard, 1835) Acanthochitona zelandica (Quoy & Gaimard, 1835) Chiton (Amaurochiton) glaucus Gray, 1828 Cryptoconchus porosus (Burrow, 1815) 69 mangrove forest ^/ salt marsh .\ / \ v m—m shell spit ^.: x x.:x.;x..x/ \ .?X \ \ \ x^x^x^ \ \ X^xi x.;.\ x. \ .\ xi:xi:xi;xi;xi:x.N x x: x 0\V.x, x x ;: x x x.: \; x x: x. x x: x x: x x. x \\x x: x x LX M X, X A. .\, X X X . XS soft mud muddy fine sand v . \ X shelly muddy fine sand muddy shelly gravel sandy fine pebble gravel cobble gravel greywacke rocks Fig. 2. Intertidal substrates and fringe communities in Te Matuku Bay, Waiheke Island. 70 m s ir or ss Ischnochiton maorianus Iredale, 1914 1 Leptochiton inquinatus (Reeve, 1847) 1 Sypharochiton pelliserpentis (Quoy & Gaimard, 1835) 1 GASTROPODA Alcithoe arabica (Gmelin, 1791) d d Amphibola crenata (Gmelin, 1791) 11 11 Buccinulum linea tinea (Martyn, 1784) 1 Buccinulum vittatum vittatum (Quoy & Gaimard, 1833) 1 Bulla quoyii Gray, 1843 d Calliostoma pellucidum (Valenciennes, 1846) d Cellana ornata (Dillwyn, 1817) Id Chemnitzia sp. I Cominella adspersa (Bruguiere, 1789) 1 I Cominella (Josepha) glandiformis (Reeve, 1847) 11 11 Cominella maculosa (Martyn, 1784) d d Cominella (Josepha) quoyana quoyana A.Adams, 1854 d Cominella (Josepha) virgata H. & A. Adams, 1853 d Cookia sulcata (Gmelin, 1791) 1 Crepidula costata Sowerby, 1824 11 Crepidula monoxyla (Lesson, 1831) Id Dicathais orbita (Gmelin, 1791) 1 Diloma (Fractarmilla) subrostrata subrostrata (Gray, 1835) 11 1 Haminoea zelandiae (Gray, 1843) d Haustrum haustorium (Gmelin, 1791) 1 1 Lepsiella scobina (Quoy & Gaimard, 1833) 11 11 Maoricolpus roseus roseus (Quoy & Gaimard, 1834) 1 d Melagraphia aethiops (Gmelin, 1791) 11 II Murexul octogonus (Quoy & Gaimard, 1833) d Neoguraleus murdochi (Finlay, 1924) d Nerita (Melanerita) atramentosa Reeve, 1855 1 Nodilittorina antipodum (Philippi, 1847) 11 11 Nodilittorina cincta (Quoy & Gaimard, 1833) I Notoacmea elongata (Quoy & Gaimard, 1834) I Notoacmea helmsi (E.A.Smith, 1894) 11 Onchidella nigricans (Quoy & Gaimard, 1832) 11 1 11 Ophicardelus costellaris (H. & A. Adams, 1854) 1 Penion sulcatus (Lamarck, 1816) d Pleurobranchaea maculata (Quoy & Gaimard, 1832) 1 Potamopyrgus estuarinus Winterbourn, 1971 Id Serpulorbis zelandicus (Quoy & Gaimard, 1834) d Sigapatella novaezelandiae (Lesson, 1831) 1 Siphonaria australis Quoy & Gaimard, 1833 1 1 71 m s ir or ss Struthiolaria papulosa (Martyn, 1784) d Struthiolaria (Pelicaria) vermis vermis (Martyn, 1784) d d Taron dubius (Hutton, 1878) d Trochus (Coelotrohus) tiaratus Quoy & Gaimard, 1834 d Trochus (Thorista) viridis Gmelin, 1791 1 Turbo smaragdus Gmelin, 1791 11 1 11 11 Xymene plebeius (Hutton, 1873) d Xymene traversi (Hutton, 1873) 1 Zeacolpus (Stiracolpus) pagoda pagoda (Reeve, 1849) d Zeacumantus lutulentus (Kiener, 1841) 1 11 Zeacumantus subcarinatus (Sowerby, 1855) 11 1 Zebittium exile (Hutton, 1873) 1 Zegalerus tenuis (Gray, 1867) d Zemitrella chaova (Reeve, 1859) d BIVALVES Anomia trigonopsis Hutton, 1877 I Arthritica bifurca (Webster, 1908) 11 d Atrina pectinata zelandica (Gray, 1835) 1 1 Austrovenus stutchburyi (Gray, 1828) 11 Cleidothaerus albidus (Lamarck, 1819) 11 Corbula (Caryocorbula) zelandica Quoy & Gaimard, 1835 1 d Crassostrea gigas (Thunberg, 1793) 11 1 11 11 Cyclomactra ovata (Gray, 1843) 1 Diplodonta (Zemysina) striatula (Finlay, 1926) d Dosina zelandica Gray, 1835 dd Dosinia (Phacosoma) subrosea (Gray, 1835) 1 d Felaniella (Zemysia) zelandica (Gray, 1835) 1 d Gari (Psammobia) lineolata (Gray, 1835) d Gari (Gobraeus) stangeri (Gray, 1843) dd Hiatella arctica (Linne, 1767) 1 lrus (Notirus) reflexus (Gray, 1843) d Leptomya retiaria retiaria (Hutton, 1885) d Limaria orientalis (A.Adams & Reeve, 1850) 1 Macomona liliana (Iredale, 1915) 11 Modiolarca impacta (Hermann, 1782) 1 Musculista senhousia (Benson, 1842) d 1 Myadora striata (Quoy & Gaimard, 1835) d Myllita (Zemyllita) stowei (Hutton, 1873) d Mytilus edulis aoteanus Powell, 1958 d Nucula hartvigiana Pfeiffer, 1864 11 d Paphies australis (Gmelin, 1791) 11 Paphies subtriangulata (Gray, 1828) d 72 m s ir or ss Pecten novaezelandiae Reeve, 1853 d Perna canaliculus (Gmelin, 1791) 1 11 Peronaea gaimardi (Iredale, 1915) d Protothaca crassicosta (Deshayes, 1835) d Ruditapes largillierti (Philippi, 1849) d Soletellina siliquens Willan, 1993 d Tawera spissa (Deshayes, 1835) d Tiostrea chilensis lutaria (Hutton, 1873) d Venericardia (Purpurocardia) purpurata (Deshayes, 1854) d Xenostrobus pulex (Lamarck, 1819) 11 11 ECHINODERMATA - ECHINOIDEA Echinocardium cordatum (Pennant, 1777) d Evechinus chloroticus (Valenciennes, 1846) 1 Fellaster zelandica (Gray, 1855) d d ASTEROIDEA Allostichaster polyplax (Muller & Troschel, 1844) 1 Coscinasterias calamaria Verrill, 1864 1 1 Patiriella regularis (Verrill, 1867) 11 1 OPHIUROIDEA Amphiocnida pilosa (Lyman, 1882) 1 Ophionereis fasciata Lutken, 1859 1 Ophiopteris antipodum Smith, 1877 1 HOLOTHUROIDEA Trochodota dendyi Mortensen, 1925 I ANNELIDA - POLYCHAETA Aedicira sp. 1 Aglaophamus macroura (Schmarda, 1861) 1 Armandia maculata (Webster, 1884) 11 Axiothella quadrimaculata Augener, 1914 1 Eteone sp. 1 Euchone sp. 11 Glycera americana Leidy, 1855 I Glycera lamelliformis Mcintosh, 1885 1 Glycera lamellipodia Knox, 1960 I Glycinde dorsalis Ehlers, 1904 11 Heteromastus sp. 11 Magelona papillicornis Muller, 1858 1 Maldanidae 11 73 m s ir or ss Nereidae 1 l Orbinia papulosa (Ehlers, 1907) 1 Paraboccardia sp. 11 Pectinaria australis Ehlers, 1904 1 Polynoidae 11 Pomatoceros caeruleus (Schmarda, 1861) 11 11 11 Prionospio sp. 11 Streblosoma
Recommended publications
  • Pineda-Salgado, 2020 CD

    Pineda-Salgado, 2020 CD

    Universidad Nacional de La Plata Facultad de Ciencias Naturales y Museo Análisis de concentraciones fósiles en la Formación Monte León (Mioceno inferior), en la costa de la provincia de Santa Cruz Gabriela Pineda Salgado Tesis doctoral Directores: Miguel Griffin, Ana Parras 2020 A mi mamá, mi abuela y mi abuelichi A Señor Pantufla y Spock-Uhura, los félidos con más estilo Agradecimientos Al Posgrado de la Facultad de Ciencias Naturales y Museo de la Universidad Nacional de La Plata. A los doctores Miguel Griffin y Ana Parras por dirigirme, por todas las facilidades brindadas para la realización de este trabajo, así como por su ayuda en las labores de campo y por los apoyos obtenidos para exponer parte de los resultados del mismo en reuniones nacionales e internacionales. Al jurado conformado por los doctores Claudia del Río, Miguel Manceñido y Sven Nielsen. A la Agencia Nacional de Promoción Científica y Tecnológica (ANPCyT) por la beca doctoral otorgada a través del Fondo para la Investigación Científica y Tecnológica (FONCyT), en el marco del Proyecto de Investigación Científica y Tecnológica PICT 2012-1726. Al Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET) por la beca interna de finalización de doctorado otorgada durante el periodo 2017-2019. Al Instituto de Ciencias de la Tierra y Ambientales de La Pampa (INCITAP, CONICET- UNLPam) y a la Facultad de Ciencias Exactas y Naturales de la UNLPam por ceder el espacio institucional para el desarrollo de esta tesis. A la Administración de Parques Nacionales por autorizar la recolección de muestras en los límites del Parque Nacional Monte León.
  • Geometric Morphometric Analysis Reveals That the Shells of Male and Female Siphon Whelks Penion Chathamensis Are the Same Size and Shape Felix Vaux A, James S

    Geometric Morphometric Analysis Reveals That the Shells of Male and Female Siphon Whelks Penion Chathamensis Are the Same Size and Shape Felix Vaux A, James S

    MOLLUSCAN RESEARCH, 2017 http://dx.doi.org/10.1080/13235818.2017.1279474 Geometric morphometric analysis reveals that the shells of male and female siphon whelks Penion chathamensis are the same size and shape Felix Vaux a, James S. Cramptonb,c, Bruce A. Marshalld, Steven A. Trewicka and Mary Morgan-Richardsa aEcology Group, Institute of Agriculture and Environment, Massey University, Palmerston North, New Zealand; bGNS Science, Lower Hutt, New Zealand; cSchool of Geography, Environment & Earth Sciences, Victoria University, Wellington, New Zealand; dMuseum of New Zealand Te Papa Tongarewa, Wellington, New Zealand ABSTRACT ARTICLE HISTORY Secondary sexual dimorphism can make the discrimination of intra and interspecific variation Received 11 July 2016 difficult, causing the identification of evolutionary lineages and classification of species to be Final version received challenging, particularly in palaeontology. Yet sexual dimorphism is an understudied research 14 December 2016 topic in dioecious marine snails. We use landmark-based geometric morphometric analysis to KEYWORDS investigate whether there is sexual dimorphism in the shell morphology of the siphon whelk Buccinulidae; conchology; Penion chathamensis. In contrast to studies of other snails, results strongly indicate that there fossil; geometric is no difference in the shape or size of shells between the sexes. A comparison of morphometrics; mating; P. chathamensis and a related species demonstrates that this result is unlikely to reflect a paleontology; reproduction; limitation of the method. The possibility that sexual dimorphism is not exhibited by at least secondary sexual some species of Penion is advantageous from a palaeontological perspective as there is a dimorphism; snail; true whelk rich fossil record for the genus across the Southern Hemisphere.
  • Nmr General (NODE87)

    Nmr General (NODE87)

    MANGELIIDAE Andonia transsylvanica (Hörnes & Auinger, 1890) NMR993000067233 Netherlands, Gelderland, Winterswijk, Miste ex coll. J.G.B. Nieuwenhuis 2 ex. FOSSIL Antiguraleus adcocki (G.B. Sowerby III, 1896) NMR993000094246 Australia, South Australia, Yorke Peninsula, Wattle Bay 1989-09-00 ex coll. H.H.M. Vermeij 33800101 1 ex. Bela antwerpiensis Marquet, 1997 NMR993000026200 Belgium, Antwerpen, Antwerpen, 6e Havendok ex coll. W.F.A. Guilonard 2 ex. FOSSIL Bela belgica (van Regteren Altena, 1959) NMR993000029020 Belgium, Antwerpen, Antwerpen ex coll. A.J. Dogterom 88263 ex. FOSSIL NMR993000026406 Belgium, Antwerpen, Antwerpen, 6e Havendok ex coll. W.F.A. Guilonard 1 ex. FOSSIL NMR993000002513 Belgium, Antwerpen, Antwerpen, raised site near Ford plant 1961-00-00 ex coll. A.W. Janssen 3 ex. FOSSIL NMR993000025608 Belgium, Antwerpen, Antwerpen, raised site near Ford plant ex coll. F.J. Janssen 20 ex. FOSSIL NMR993000002092 Belgium, Oost-Vlaanderen, Tielrode, Groeve N.V. Tielrode & Stekene ex coll. Maarten van den Bos 1 ex. FOSSIL NMR993000028678 Netherlands, Zeeland, Westerschelde, shell bank off Ellewoutsdijk at 5-10 m depth 1939-00-00 ex coll. A.J. Dogterom 51 ex. FOSSIL Bela consimilis Harmer, 1915 NMR993000025704 Netherlands, Zeeland, Walcheren, Veere, Domburg 1951-09-00 ex coll. N.P.W. Balke 2 ex. FOSSIL NMR993000025633 Netherlands, Zeeland, Westerschelde, shell bank off Ellewoutsdijk at 5-10 m depth ex coll. W.F.A. Guilonard 166b1 ex. FOSSIL NMR993000025658 Netherlands, Zeeland, Westerschelde, shell bank off Ellewoutsdijk at 5-10 m depth 1949-06-00 ex coll. N.P.W. Balke 1 ex. FOSSIL Bela cycladensis (Reeve, 1845) NMR993000075371 Cyprus, Famagusta, Famagusta Bay, Ayios Seryios 2012-11-00 ex coll.
  • Phylum MOLLUSCA Chitons, Bivalves, Sea Snails, Sea Slugs, Octopus, Squid, Tusk Shell

    Phylum MOLLUSCA Chitons, Bivalves, Sea Snails, Sea Slugs, Octopus, Squid, Tusk Shell

    Phylum MOLLUSCA Chitons, bivalves, sea snails, sea slugs, octopus, squid, tusk shell Bruce Marshall, Steve O’Shea with additional input for squid from Neil Bagley, Peter McMillan, Reyn Naylor, Darren Stevens, Di Tracey Phylum Aplacophora In New Zealand, these are worm-like molluscs found in sandy mud. There is no shell. The tiny MOLLUSCA solenogasters have bristle-like spicules over Chitons, bivalves, sea snails, sea almost the whole body, a groove on the underside of the body, and no gills. The more worm-like slugs, octopus, squid, tusk shells caudofoveates have a groove and fewer spicules but have gills. There are 10 species, 8 undescribed. The mollusca is the second most speciose animal Bivalvia phylum in the sea after Arthropoda. The phylum Clams, mussels, oysters, scallops, etc. The shell is name is taken from the Latin (molluscus, soft), in two halves (valves) connected by a ligament and referring to the soft bodies of these creatures, but hinge and anterior and posterior adductor muscles. most species have some kind of protective shell Gills are well-developed and there is no radula. and hence are called shellfish. Some, like sea There are 680 species, 231 undescribed. slugs, have no shell at all. Most molluscs also have a strap-like ribbon of minute teeth — the Scaphopoda radula — inside the mouth, but this characteristic Tusk shells. The body and head are reduced but Molluscan feature is lacking in clams (bivalves) and there is a foot that is used for burrowing in soft some deep-sea finned octopuses. A significant part sediments. The shell is open at both ends, with of the body is muscular, like the adductor muscles the narrow tip just above the sediment surface for and foot of clams and scallops, the head-foot of respiration.
  • Molluscs 2018 Program and Abstract Handbook

    Molluscs 2018 Program and Abstract Handbook

    © Malacological Society of Australia 2018 Abstracts may be reproduced provided that appropriate acknowledgement is given and the reference cited. Requests for this book should be made to: Malacological Society of Australia information at: http://www.malsocaus.org/contactus.htm Program and Abstracts for the 2018 meeting of the Malacological Society of Australasia (2nd to 5th December, Wellington, New Zealand) Cover Photo and Design: Kerry Walton Logo Design: Platon Vafiadis Compilation and layout: Julie Burton, Carmel McDougall and Kerry Walton Publication Date: November 2018 Recommended Retail Price: $25.00 AUD Malacological Society of Australasia, Triennial Conference Table of contents The Conference Venue ................................................................................................................... 3 Venue floorplan ............................................................................................................................. 3 General Information ....................................................................................................................... 4 Molluscs 2018 Organising Committee ............................................................................................. 6 Our Sponsors .................................................................................................................................. 6 MSA Annual General Meeting and Election of Office Bearers ......................................................... 7 President’s Welcome .....................................................................................................................
  • Marine Mollusca of Isotope Stages of the Last 2 Million Years in New Zealand

    Marine Mollusca of Isotope Stages of the Last 2 Million Years in New Zealand

    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/232863216 Marine Mollusca of isotope stages of the last 2 million years in New Zealand. Part 4. Gastropoda (Ptenoglossa, Neogastropoda, Heterobranchia) Article in Journal- Royal Society of New Zealand · March 2011 DOI: 10.1080/03036758.2011.548763 CITATIONS READS 19 690 1 author: Alan Beu GNS Science 167 PUBLICATIONS 3,645 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Integrating fossils and genetics of living molluscs View project Barnacle Limestones of the Southern Hemisphere View project All content following this page was uploaded by Alan Beu on 18 December 2015. The user has requested enhancement of the downloaded file. This article was downloaded by: [Beu, A. G.] On: 16 March 2011 Access details: Access Details: [subscription number 935027131] Publisher Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37- 41 Mortimer Street, London W1T 3JH, UK Journal of the Royal Society of New Zealand Publication details, including instructions for authors and subscription information: http://www.informaworld.com/smpp/title~content=t918982755 Marine Mollusca of isotope stages of the last 2 million years in New Zealand. Part 4. Gastropoda (Ptenoglossa, Neogastropoda, Heterobranchia) AG Beua a GNS Science, Lower Hutt, New Zealand Online publication date: 16 March 2011 To cite this Article Beu, AG(2011) 'Marine Mollusca of isotope stages of the last 2 million years in New Zealand. Part 4. Gastropoda (Ptenoglossa, Neogastropoda, Heterobranchia)', Journal of the Royal Society of New Zealand, 41: 1, 1 — 153 To link to this Article: DOI: 10.1080/03036758.2011.548763 URL: http://dx.doi.org/10.1080/03036758.2011.548763 PLEASE SCROLL DOWN FOR ARTICLE Full terms and conditions of use: http://www.informaworld.com/terms-and-conditions-of-access.pdf This article may be used for research, teaching and private study purposes.
  • Mollusca Gastropoda : Columbariform Gastropods of New Caledonia

    Mollusca Gastropoda : Columbariform Gastropods of New Caledonia

    ÎULTATS DES CAMPAGNES MUSORSTOM. VOLUME 7 RÉSULTATS DES CAMPAGNES MUSORSTOM. VOLUME i RÉSUI 10 Mollusca Gastropoda : Columbariform Gastropods of New Caledonia M. G. HARASEWYCH Smithsonian Institution National Museum of Natural History Department of Invertebrate Zoology Washington, DC 20560 U.S.A. ABSTRACT A survey of the deep-water malacofauna of New Caledo­ Fustifusus. Serratifusus virginiae sp. nov. and Serratifusus nia has brought to light two species referable to the subfamily lineatus sp. nov., two Recent species of the columbariform Columbariinac (Gastropoda: Turbincllidae). Coluzca faeeta genus Serratifusus Darragh. 1969. previously known only sp. nov. is described from off the Isle of Pines at depths of from deep-water fossil deposits of Miocene age. arc also 385-500 m. Additional specimens of Coluzea pinicola Dar- described. On the basis of anatomical and radular data, ragh, 19X7, previously described from off the Isle of Pines, Serratifusus is transferred from the Columbariinae to the serve as the basis for the description of the new genus family Buccinidae. RESUME Mollusca Gastropoda : Gastéropodes columbariformes de également décrite de l'île des Pins, a été récoltée vivante et Nouvelle-Calédonie. devient l'espèce type du nouveau genre Fustifusus. Le genre Serratifusus Darragh. 1969 n'était jusqu'ici connu que de Au cours des campagnes d'exploration de la faune pro­ dépôts miocènes en faciès profond : deux espèces actuelles. .S. fonde de Nouvelle-Calédonie, deux espèces de la sous-famille virginiae sp. nov. et S. lineatus sp. nov., sont maintenant Columbariinae (Gastropoda : Turbinellidae) ont été décou­ décrites de Nouvelle-Calédonie. Sur la base des caractères vertes. Coluzea faeeta sp.
  • Gastropoda, Buccinidae), a Reappraisal

    Gastropoda, Buccinidae), a Reappraisal

    Beets, Notes on Buccinulum, a reappraisal, Scripta Geol., 82 (1986) Notes on Buccinulum (Gastropoda, Buccinidae), a reappraisal C. Beets Beets, C. Notes on Buccinulum (Gastropoda, Buccinidae), a reappraisal. — Scripta Geol., 82: 83-100, pis 6-7, Leiden, January 1987 An attempt was made to assemble what is known at present of Buccinulum in the Indo-Western Pacific Region, fossil and Recent, more scope being offered by the discovery of new Miocene fossils from Java and Sumatra, and the recognition of further fossil species from India and Burma. This induced comparisons with, and revisions of some of the fossil and living species occurring in adjacent zoogeographical provinces. The Recent distribution of the subgenus Euthria appears to be much more extensive than when recorded by Wenz (1938-1944), the minimum enlargement encompassing an area stretching from the eastern Indian Ocean to Japan, via the Philippines and Ryukyu Islands. The knowledge of its fossil distribution, in the Indopacific Region long confined to Javanese Eocene, has likewise greatly expanded by discoveries made in Neogene to Quaternary of India, Burma, Indonesia (Sumatra, Java, Madura, and Borneo), the Philippines, New Hebrides, Fiji?, Ryukyu Islands, and Japan. The relevant data were tabulated. New taxa described are: Buccinulum pendopoense and B. sumatrense, both from presumed Preangerian of Sumatra, and B. walleri sedanense from the Rembangian of Java. It is proposed to include Ornopsis, which was described from the Upper Cretaceous of North America, as a subgenus of Buccinulum. It may well be ancestral to Euthria, considering its similarity to certain of the latter's fossil and living species.
  • New Buccinoid Gastropods from Uppermost Cretaceous and Paleocene Strata of California and Baja California, Mexico

    New Buccinoid Gastropods from Uppermost Cretaceous and Paleocene Strata of California and Baja California, Mexico

    THE NAUTILUS 120(2):66–78, 2006 Page 66 New buccinoid gastropods from uppermost Cretaceous and Paleocene strata of California and Baja California, Mexico Richard L. Squires LouElla R. Saul Department of Geological Sciences Invertebrate Paleontology Section California State University, Natural History Museum of Los Angeles Northridge, CA 91330–8266 USA County [email protected] 900 Exposition Boulevard Los Angeles, CA 90007 USA [email protected] ABSTRACT better understanding of the relationship between Ornop- sis? n. sp. and “T.” titan. Saul’s Ornopsis? n. sp. is herein Two new genera and three new species of extinct buccinoid assigned to Ornopsis? dysis new species, and its genus gastropods are described and named from the Pacific slope of assignment cannot be made with certainty until more North America. The buccinid? Ornopsis? dysis new species is specimens are found. Ornopsis sensu stricto Wade, 1916, from uppermost Maastrichtian (uppermost Cretaceous) strata heretofore has been reported with certainty only from in the Dip Creek area, San Luis Obispo County, west-central Upper Cretaceous (upper Campanian to upper Maas- California. The fasciolarine fasciolarid? Saxituberosa new genus is comprised of the lineage Saxituberosa fons new species, from trichtian) strata of the southeastern United States (Sohl, lower Paleocene (Danian) strata in Los Angeles County, south- 1964). “Trachytriton” titan is herein found to occur in ern California, and Saxituberosa titan (Waring, 1917), from middle Paleocene strata in southern California. Its char- middle Paleocene (Selandian) strata in Ventura and Los Ange- acteristics separate it from the cymatiid Trachytriton les counties, southern California, and northern Baja California, Meek, 1864, and “T.” titan is assigned to Saxituberosa Mexico.
  • Ahipara, Herekino April 1999, Molluscan Biogeographic

    Ahipara, Herekino April 1999, Molluscan Biogeographic

    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/256555636 Intertidal biota and washup at Ahipara and Herekino, Northland west coast. Article · January 2004 CITATIONS READS 0 101 7 authors, including: Bruce W Hayward Margaret S. Morley Geomarine Research Auckland Museum 675 PUBLICATIONS 4,416 CITATIONS 58 PUBLICATIONS 355 CITATIONS SEE PROFILE SEE PROFILE Wilma Blom Auckland Museum 18 PUBLICATIONS 311 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: MSc research - Pleistocene extinctions of deep-sea benthic foraminifera: the South Atlantic record View project All content following this page was uploaded by Bruce W Hayward on 06 February 2014. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. INTERTIDAL BIOTA AND WASHUP AT AHIPARA AND HEREKINO, NORTHLAND WEST COAST Bruce W. Hayward1, Margaret S. Morley2, Hugh R. Grenfell1, Rowan Carter3, Glenys C. Hayward4, Wilma M. Blom2, Doug Rogan5 1Geomarine Research, 49 Swainston Rd, St Johns, Auckland, 2Auckland War Memorial Museum, Private Bag 92018, Auckland, 3North Shore City Council, Auckland, 419 Debron Ave, Remuera, Auckland,5Canterbury Museum, Christchurch SUMMARY Three hundred and twenty-nine species are recorded from the Ahipara and Herekino Harbour shores of north-west Northland. These include 178 species of gastropods, 56 species of bivalves, 29 species of seaweeds, 14 species of crabs, 10 species each of chitons and barnacles, 9 species of echinoderms, 6 species each of anemones and polychaete worms.
  • Title Evolution of the Gastropod Genus Siphonalia with Accounts on The

    Title Evolution of the Gastropod Genus Siphonalia with Accounts on The

    Evolution of the Gastropod Genus Siphonalia with accounts on Title the Pliocene Species of Tōtōmi and other Examples : The Ketienzian Fauna Series, no. 1 Author(s) Makiyama, Jiro Memoirs of the College of Science, Kyoto Imperial University. Citation Ser. B (1941), 16(2): 75-93 Issue Date 1941-03-31 URL http://hdl.handle.net/2433/257908 Right Type Departmental Bulletin Paper Textversion publisher Kyoto University MEMolRs eF Tf{E COLLEGE OF S:IENCE,KyoTe ZMpERiALUNIVERSITY,SERrEs B, VoL. XVI, N'o. 2, ART. 4, 1941. Evolutien'of the Gastroped Genus Siphonalia with accounts on the Pliocene Species of T6t6mi and other Examvles The Ketlenzian Fauna Series, no. 1 By Jir6 MAKIYAMA With 4 Ptates and 4 Test-fi.crares (Received 7, November1939) First Words to the Ketienzian Fauna Series The work on the Tertiary stratigraphy and palaeontology of the areas in T6t6mi was undertaken by myself from 1919, and its outcome was partly made public, two in English (this Memoirs, B-3, art. 1, B-, art. 1.) aRd others in our language. Iam still working on the same field as it takes very irnportant place in the geology of this laftd. In the first Eng!ish paper, details of the Mollusca of the Dainitian stage or the Lower Kakegawa forma- tion have been given. In comparison with the DaiRitian fauna, the Ketienzian or the Upper Kakegawa fauna was seemingly very poor, for the beds were deposited under the sea deeper than that of the Dainitian. From the Hosoya beds which are the representative of the lowest level of the age, some small number of Mollttsca was listed in the second English paper.
  • Conradconfusus, a Replacement Name for Buccinofusus

    Conradconfusus, a Replacement Name for Buccinofusus

    Cainozoic November 2002 Research, 1(1-2) (2001), pp. 129-132, a name for Conradconfusus, replacement Buccinofusus Conrad, 1868, non 1866 (Mollusca, Gastropoda) Martin+Avery Snyder Research Associate, Department of Malacology, Academy of Natural Sciences ofPhiladelphia, 19th and Benjamin Franklin Park- PA way, Philadelphia, 19103, USA; e-mail: [email protected] Received 6 August 2002; revised version accepted 20 August 2002 The Fusus is for new genus Conradconfusus n. gen., type species parilis Conrad, 1832, proposed as a replacement name Buccinofu- 1868 strata sus Conrad, (non 1866). Twenty-three (sub)species, from Upper Cretaceous and Cainozoic worldwide, may be assigned this to genus. Key words: Mollusca, Gastropoda, Cretaceous, Cainozoic, replacement name, lectotype. Introduction diegoensis and Fusus parilis are not congeneric, and the latter use of the genus name Buccinofusus, probably in Conrad introduced the (1866, p. 17) validly genus Bucci- the neogastropod family Fasciolariidae, requires re- nofusus by the combination Buccinofusus diegoensis placement. (Gabb); the type species, by monotypy, being Tritonium diegoensis Gabb, 1864 (p. 95, pi. 18, fig. 44) from the Eocene of California. The nearly complete holotype, A replacement name which is 14.3 mm in height and 8.5 mm in width, was reported by Stewart (1927, p. 430) to be in the Museum When Conrad (1868) introduced Buccinofusus, he sug- of Paleontology at Berkeley, California (registration gested four possible species as members of this genus, in number 11980). The was noted by Stewart (1927, addition to F. parilis viz. genus , but overlooked Neave p. 430) by (1939-1966). Vaught (1989, p. 50) listed the genus Buccinofusus with the date Buccinum balteatumReeve, 1846 (Recent, Australia); 1866.